On the deep general circulation in the western North Atlantic
On the deep general circulation in the western North Atlantic
dc.contributor.author | Schmitz, William J. | |
dc.date.accessioned | 2018-09-24T17:33:28Z | |
dc.date.available | 2018-09-24T17:33:28Z | |
dc.date.issued | 1978-04 | |
dc.description | Also published as: Journal of Marine Research, Volume 35, 1977, pp. 21-28 | en_US |
dc.description.abstract | Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the vicinity of a recently hypothesized (Worthington, in press) horizontally restricted subtropical gyre in the deep western North Atlantic. The Reynolds stresses associated with low frequency fluctuations may play a significant role in the dynamics of this deep mean flow, possibly inducing a significant downstream increase in transport of the Gulf Stream, perhaps driving the deep gyre. | en_US |
dc.description.sponsorship | Prepared for the Office of Naval Research under Contracts N00014-66-C-0241; NR 083- 004 and N00014-74-C-0262; NR 083-004 and for the International Decade of Ocean Exploration of the National Science Foundation under Grant OCE75-03962. | en_US |
dc.identifier.citation | Schmitz, W. J. (1978). On the deep general circulation in the western North Atlantic. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/10589 | |
dc.identifier.doi | 10.1575/1912/10589 | |
dc.identifier.uri | https://hdl.handle.net/1912/10589 | |
dc.language.iso | en_US | en_US |
dc.publisher | Woods Hole Oceanographic Institution | en_US |
dc.relation.ispartofseries | WHOI Technical Reports | en_US |
dc.relation.ispartofseries | WHOI-78-3 | en_US |
dc.subject | Ocean circulation | en_US |
dc.title | On the deep general circulation in the western North Atlantic | en_US |
dc.type | Technical Report | en_US |
dspace.entity.type | Publication | |
relation.isAuthorOfPublication | 5412bdba-589d-42ee-aa92-611d19722472 | |
relation.isAuthorOfPublication.latestForDiscovery | 5412bdba-589d-42ee-aa92-611d19722472 |